With the growth of interest in global warming in the 1980s came renewed interest in the past temperature record, and the question of whether past times had been warmer or colder than "present". However, at that time available records were few. The discussion in chapter 7 "Observed climate variations and change" of the last 1000 years (excluding the instrumental period) occupies less than a page.

A schematic (non-quantitative) curve was used to represent temperature variations over the last 1000 years in chapter 7. The vertical temperature scale was labelled as "Temperature change (°C)" but no numerical labels were given; it could be taken to imply that temperature variations of the MWP and LIA were each of the order of 0.5 °C from the temperature around 1900. The section specifically states recent climate changes were in a range of probably less than 2 °C. The 1990 report noted that it was not clear whether all the fluctuations indicated were truly global (p 202). The graph had no clear source (but can be traced to publications by Hubert Lamb representing the Central England Temperature; those publications have no explicit calibration against instrumental data, [and are] just Lamb’s qualitative judgement and interpretation of what he refers to as the ‘evidence’[1]), and disappeared from the 1992 supplementary report.

Within the 1990 report, the LIA is taken to be global in extent but the MWP is not. Climate over the last 1000 years is mentioned very briefly in the SPM of the 1990 report. The MWP is not mentioned at all, and the LIA described by ...probably fluctuated by little more than 1°C. Some fluctuations lasted several centuries, including the LIA which ended in the [19th century] and which appears to have been global in extent. The MWP is mentioned in the executive summary to chapter 7, as MWP around 1000 AD (which may not have been global).

The 1992 report (appendix C) used only two graphs of pre-instrumental temperatures, from (Wang and Wang 1991). They show air temperature based on documentary evidence in East and North China from 1350 to 1950. Fluctuations are of the order of 0.5-0.75 °C and indicate, variably, colder-than-present temperatures before the 20th century. The graph stops in 1350 and does not show a MWP. The only text reference to the MWP is qualified by in this region in boldface.

By 1995, research in the subject had advanced and hemispherical reconstructions of temperature were available, though only for the summer season (because tree rings are often most strongly influenced by summer temperatures). The 1995 IPCC report used a northern hemisphere summer temperature reconstruction (fig 3.20) from 1400 to 1979 by (Bradley and Jones 1993). This too shows no MWP (it only goes back to 1400) and colder temperatures otherwise before the 20th century, of the order of 0.5 °C colder. Fig 3.21 shows 8 ice core records from 1200 to present, which display a mixed pattern.

The MWP and LIA are introduced, in the text, as "two periods which have received special attention... These have been interpreted, at times, as periods of global warmth and coolness, respectively. Recent studies have re-evaluated the interval commonly known as the Medieval Warm Period to assess the magnitude and geographical extent of any prolonged warm interval between the 9th and 14th centuries (Hughes and Diaz, 1994). The available evidence is limited (geographically) and is equivocal." After discussing the evidence, it concluded "a clearer picture may emerge as more and better calibrated proxy records are produced. However, at this point, it is not yet possible to say whether, on a hemispheric scale, temperatures declined from the 11-12th to the 16-17th century. Nor, therefore, is it possible to conclude that global temperatures in the Medieval Warm Period were comparable to the warm decades of the late 20th century."

The IPCC TAR says of the MWP that the posited Medieval Warm Period appears to have been less distinct, more moderate in amplitude, and somewhat different in timing at the hemispheric scale than is typically inferred for the conventionally defined European epoch. The Northern Hemisphere mean temperature estimates of (Jones et al. 1998), (Mann et al. 1999), and (Crowley & Lowery 2000) show temperatures from the 11th to 14th centuries to be about 0.2°C warmer than those from the 15th to 19th centuries, but rather below mid-20th century temperatures.[3]

The TAR discusses Was there a "Little Ice Age" and a "Medieval Warm Period"? and says Thus current evidence does not support globally synchronous periods of anomalous cold or warmth over this timeframe, and the conventional terms of "Little Ice Age" and "Medieval Warm Period" appear to have limited utility in describing trends in hemispheric or global mean temperature changes in past centuries.[3]

The 2007 report used more recent temperature reconstructions including (Esper et al. 2002), (Bradley et al. 2003a), (Jones and Mann 2004), (D’Arrigo et al. 2006). The IPCC concluded the warmest period prior to the 20th century very likely occurred between 950 and 1100...The evidence currently available indicates that NH mean temperatures during medieval times (950–1100) were indeed warm in a 2-kyr context and even warmer in relation to the less sparse but still limited evidence of widespread average cool conditions in the 17th century (Osborn & Briffa 2006). However, the evidence is not sufficient to support a conclusion that hemispheric mean temperatures were as warm, or the extent of warm regions as expansive, as those in the 20th century as a whole, during any period in medieval times (Jones et al., 2001; Bradley et al., 2003a,b; Osborn & Briffa 2006).[4]

AR5 prefers the term "Medieval Climate Anomaly" (MCA) to "Medieval Warm Period". Chapter 5, section 5.3.5.1 discussed work since AR4 on the MCA and LIA. It notes that the timing and spatial structure of the MCA and LIA are complex, with different reconstructions exhibiting warm and cold conditions at different times for different regions and seasons. A combination of NH temperature reconstructions shows mostly warm conditions from about 950 to about 1250 and colder conditions from about 1450 to about 1850, which are taken to represent the times of the MCA and LIA.

They express high confidence that the mean NH temperature of the last 30 or 50 years exceed 30- or 50-year means of the past 800 years, and medium confidence that the last 30 years were likely the warmest 30-year period of the last 1400 years.[5]